Nova Hedwigia
83 3—4
431—449
Stuttgart, November 2006
New records of Trentepohliales
(Ulvophyceae, Chlorophyta) from Africa
by
Fabio Rindi*1, Michael D. Guiry2 and Juan M. López-Bautista1
1
2
Department of Biological Sciences, The University of Alabama, P.O. Box 870345,
425 Scientific Collections Building, Tuscaloosa, AL 35487-0345, U.S.A.
AlgaeBase Centre, Martin Ryan Institute, National University of Ireland, Galway, Ireland
With 31 figures
Rindi, F., M.D. Guiry & J.M. López-Bautista (2006): New records of Trentepohliales (Ulvophyceae,
Chlorophyta) from Africa. - Nova Hedwigia 83: 431-449.
Abstract: The diversity and distribution of the Trentepohliales have been investigated in detail in
several regions of Europe and Asia. However, the information available for other continents is
relatively limited and very little is known for these algae in Africa. New records of Trentepohliales
for Africa were obtained in the course of surveys conducted in 2005 in South Africa, Namibia and
Tanzania. For Phycopeltis epiphyton, Trentepohlia abietina and Trentepohlia flava, these are the first
documented records for the continent. A species of Printzina, probably an undescribed taxon, was
collected from trees in Tanzania. The new collections allowed the rediscovery and characterization of
some poorly known species, of dubious taxonomic validity, such as Trentepohlia afra and T. chinensis.
Additional records of widespread species, such as Phycopeltis arundinacea and Trentepohlia umbrina,
were also obtained. The morphology and distribution of the species collected are described and the
taxonomic and biogeographical implications of the new records are discussed.
Introduction
The order Trentepohliales includes subaerial green algae widespread in tropical and
temperate regions with humid climates, where they occupy a wide range of habitats
and occur on a great range of substrata (Chapman 1984; Ettl & Gärtner 1995;
Thompson & Wujek 1997). This order is distinguished from all other green algae by
the unique combination of the following features: presence of β-carotene and
haematochrome (which colour the thallus yellow, orange or red), absence of pyrenoids
in the chloroplast, a unique flagellar apparatus, transverse cell walls with
*Author to whom correspondence should be addressed; e-mail: frindi@bama.ua.edu
DOI: 10.1127/0029-5035/2006/0083-0431
0029-5035/06/0083-0431 $ 4.75
© 2006 J. Cramer in der Gebrüder Borntraeger
Verlagsbuchhandlung, D-14129 Berlin · D-70176 Stuttgart
431
plasmodesmata, and presence of a unique reproductive structure, the sporangiate
lateral. The sporangiate lateral is a highly modified branch; it consists of an apical
cell (the suffultory cell) that is swollen basally and tapers apically into a short neck,
on which a spherical or oval zoosporangium is borne (Fig. 1). At maturity, the
zoosporangium is shed and carried by the wind, contributing to the dispersal of these
algae. Due to such unusual combination of features, the position of the Trentepohliales
at the class level has been long uncertain (Chapman et al. 2001; López-Bautista et al.
2002). Only recently, molecular data have provided conclusive evidence that the
Trentepohliales are members of the class Ulvophyceae (López-Bautista & Chapman
2003). However, despite more than 200 years of intensive study, the taxonomy at
genus and species level is still affected by many unsolved problems. As presently
circumscribed, the order includes five genera: Cephaleuros Kunze ex Fries 1832,
Phycopeltis Millardet 1870, Printzina Thompson & Wujek 1992, Stomatochroon
Palm 1934 and Trentepohlia Martius 1817 (the taxonomic validity of Physolinum
Printz 1920 is controversial and, in the recent literature, this genus has generally not
been separated from Trentepohlia). Although the morphological separation of the
genera is straightforward, recent evidence based on SSU rRNA sequences suggests
that the characters traditionally used for the separation at the genus level have no
phylogenetic significance, and a radical revision of the generic arrangement of the
group will be probably necessary (López-Bautista et al. 2006). Delimitation at the
species level is also often difficult. To date, species-level identification in the
Trentepohliales is almost entirely based on gross morphology, which in some species
is known to encompass considerable variation. Several species of Trentepohlia and
Printzina, the genera most intensively studied, are reported to be very polymorphic
(Hariot 1889a; Printz 1920, 1939; Rindi & Guiry 2002a). Although for the typical
forms of most species the identification is relatively straightforward, not infrequently
field-collected specimens show an intermediate morphology and are difficult or
impossible to identify unambiguously. The distinction of species of Cephaleuros and
Phycopeltis is often based on subtle characters, for which the range of variation is
poorly understood (e.g., Rindi & Guiry 2002b; Neustupa 2005). Furthermore,
descriptions and illustrations available for several species in the main taxonomic
treatments of this group are poor and inadequate, since failing to depict or describe
some important characters. For these reasons, basic investigations on the diversity
and ecology of these algae should be considered still very valuable, especially when
they provide new information for geographical areas for which little or nothing is
known (Rindi et al. 2005).
For historical reasons, Europe and some parts of Asia are the regions for which
the diversity of the Trentepohliales has been studied best. Relatively recently,
several studies have provided important contributions for North and Central
America (Dillard 1989; Thompson & Wujek 1997; John 2003), South America
(Akiyama 1971; Tracanna 1989), Australia (Cribb 1958, 1963, 1964, 1968, 1970),
New Zealand (Sarma 1986) and the Pacific islands (Brooks 2004; Rindi et al.
2005). There is no doubt that, to date, Africa is the continent for which by far
the least is known about the Trentepohliales. Some taxa were described for material
collected on this continent in the 19th century (Montagne 1846, Reinsch 1877,
Hariot 1893). In a study of subaerial algae from Natal, South Africa, Printz
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Fig. 1. Structure of the sporangiate lateral.
(1920) reported records of several species of Phycopeltis and Trentepohlia, with
a detailed description of their morphology. Flint (1959) described the growth
and reproduction in culture of a strain of Physolinum monile (De Wildeman)
Printz from Nigeria. Apart for these studies, the information available for African
Trentepohliales is extremely limited and fragmentary. Other records of
Trentepohlia are available for Algeria, Congo, Morocco and South Africa (Hariot
1891, 1913, Feldmann 1947, Gauthier-Lièvre 1954, Woodhead & Tweed 1958,
Joska & Bolton 1996). Records of Cephaleuros have been reported by Thompson
& Wujek (1997) for Cameroon, Kenya, South Africa and Tanzania. However,
these records usually include very few or no details on morphology and ecology;
Thompson & Wujek’s (1997) records are part of more general treatments and no
details specific to the African material are included. In this paper, we report on
some Trentepohliales collected in the course of trips to several African localities
in 2005. These collections led to the discovery of several interesting taxa. Since
some of these have been poorly characterized in the previous literature, we believe
that accurate descriptions and illustrations will be very helpful for comparative
purposes. Some of the species recorded have not been previously reported for
Africa; for an entity attributable to Printzina, the morphology does not match
any of the species currently attributed to the genus and there is the possibility
that this might represent an undescribed species. For each entity, morphology
and ecology are described in detail and the taxonomic and biogeographical
implications of the records are discussed.
433
Materials and methods
Collections were made at several locations in separate trips. Samples from Zanzibar, Tanzania, were
collected by one of us (MDG) in April 2005, mainly from bark of trees and leaves. A large set of
samples from several localities in the provinces of Western Cape and Eastern Cape, South Africa,
was obtained by the same collector in September-October 2005; in this case, samples were also
collected from natural rocks and artificial surfaces (painted concrete). Collections from tree bark
were made by JMLB in the province of Kwa-Zulu Natal in August 2005. Finally, a collection
obtained from bark and leaves of coastal trees at Swakopmund, Namibia, in July 2005, was kindly
supplied by Dr Willem Prud’homme van Reine (Rjiksherbarium Leiden, the Netherlands). Collection
details are reported for each entity recorded. Due to the exotic nature of the host plants to the authors,
the brief duration of the trips and the lack of local colleagues able to provide identification, for
collections obtained from leaves and tree bark the host plants could not be determined. Voucher
specimens are deposited in the Phycological Herbarium, National University of Ireland, Galway
(GALW). The material was examined by light microscopy. Microphotographs were taken by a
Nikon DXM1200 digital camera and mounted in plates using Adobe Photoshop CS (version 8.0). A
larger set of photographs of the species collected is available in AlgaeBase (www.algaebase.org).
Results and discussion
Phycopeltis arundinacea (Montagne) De Toni
This species occurred on leaves of several tree species in Nature’s Valley, Tsitsikamma
National Park and Robberg Nature Reserve, South Africa, in September 2005. At Robberg,
specimens were also found on a plastic tree label. Specimens growing freely consisted of
rounded disks (Fig. 2), with a regular smooth margin (Fig. 3), and were up to 1.5 mm in
diameter. When the margins of two individual specimens met, they stopped growing in the
area of contact and their growth continued in other directions; this produced thalli with an
irregular outline. Vegetative cells were 8-17 µm long (mainly 10-13) and 5-12 µm wide
(mainly 7.5-9.0), the length:width ratio ranging between 1 and 2.5 (mainly ~ 1.5).
Sporangiate laterals occurred on most specimens examined. They were produced randomly
in the central parts of the thallus, in intercalary position, and were absent in the marginal
parts. The sporangiate laterals were formed by an oval zoosporangium occurring at the top
of a suffultory cell with a retorted neck. The suffultory cells were produced directly from
vegetative cells and there was no evidence of production of a stalk cell or a sporangiophore
(Fig. 4). The zoosporangium was 12-20 µm wide and 15-25 µm long; the ostiole was
opposite to the attachment of the sporangium (Fig. 5). Mature gametangia were not seen
with any certainty. In several large thalli, however, many discoloured cells occurred in the
central parts. These might have been empty gametangia that had discharged gametes; this,
however, could not be confirmed since these parts were frequently invaded by fungal
hyphae, which made observation difficult, and no ostioles could be observed with certainty.
Figs 2-9. Phycopeltis arundinacea and Phycopeltis epiphyton. Figs 2-5. Phycopeltis arundinacea.
Fig. 2. Habit (scale = 100 µm). Fig. 3. Detail of margin (scale = 50 µm). Fig. 4. Surface view of
thallus, with some zoosporangia in development (scale = 20 µm). Fig. 5. Detail of a mature zoosporangium (scale = 20 µm). Figs 6-9. Phycopeltis epiphyton. Fig. 6. Habit of a young specimen (scale
= 30 µm). Fig. 7. A mature, reproductive specimen (scale = 40 µm). Fig. 8. Detail of thallus with
gametangia (scale = 20 µm). Fig. 9. Detail of gametangia after release of gametes; note ostioles
(arrowheads) (scale = 10 µm).
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435
Phycopeltis arundinacea has been reported for several regions of Europe and Asia,
both temperate and tropical (see Rindi et al. 2004 and Neustupa 2005, for a summary
of the geographical distribution). Thompson & Wujek (1997) mentioned that
Phycopeltis arundinacea is also present in the New World tropics; however, the
taxonomic identity of the material that they referred to this species is not clear, as the
description that they provided for it is not in complete agreement with the morphology
of the type material (see discussion in Rindi & Guiry 2002b, Rindi et al. 2004 and
Neustupa 2005). Apart for the original description from Algeria (Montagne 1846, as
Phyllactidium arundinaceum), at present the only documented record for Africa is
that of Printz (1920) from Saldanha Bay, on the west coast of South Africa, and
from the environs of Durban, Kwa-Zulu Natal, South Africa. In the present collections,
we could not observe with certainty gametangia, which are reported to occur on
thalli that also produce sporangiate laterals in collections from other regions (Rindi
& Guiry 2002b; Neustupa 2003; Rindi et al. 2003; Neustupa 2005). However, the
morphology of the material is in good agreement with collections of Phycopeltis
arundinacea from several locations in Europe (Rindi & Guiry 2002b, Rindi et al.
2003, 2004) and is characterized by a combination of characters that allow it to be
discriminated from similar species, such as Phycopeltis expansa Jennings (Jennings
1895), P. novae-zelandiae Thompson & Wujek (Thompson & Wujek 1997),
P. theaensis Neustupa (Neustupa 2003) and P. javanica Neustupa (Neustupa 2005).
It seems therefore reasonable to refer the present collections to this species.
Phycopeltis epiphyton Millardet
Specimens attributable to this species formed a fine, dense cover on leaves of some
shrubs and trees in Tsitsikamma National Park and Robberg Nature Reserve, South
Africa, in September 2005. The normal shape of individual thalli was rounded or
polygonal, with entire margins (Fig. 6); specimens were up to 150-160 µm in diameter.
The material examined formed very crowded populations on the leaves on which this
species occurred. Relatively large portions of leaves were covered by an extensive
layer formed by many joined specimens. Growth stopped when the margin of a thallus
came into contact with neighbouring thalli and continued in directions where space
was available; in this way, many specimens assumed an irregular outline. In most
thalli, the central parts were formed by empty gametangia and living vegetative cells
occurred only in the marginal parts (Fig. 7). Vegetative cells were 4-8 µm wide (mainly
5-7) and 8-15 µm long (mainly 9-11). Gametangial specimens started to become
reproductive when the thallus reached a diameter of 60-70 µm; the cells situated in the
centre of the thallus became gametangia and released gametes (Fig. 8). This pattern
extended gradually to more peripheral parts of the thallus. Mature gametangia were
globular or polygonal, 12-18 µm in diameter; the ostiole was produced in a corner of
the gametangium (Fig. 9). No sporangiate laterals were observed.
Phycopeltis epiphyton is the type species of the genus and is reported as pantropical (Thompson
& Wujek 1997); however, this is the first documented record for Africa. The morphology of
the material from South Africa is in good agreement with the original description of this
species from the Black Forest, Germany (Millardet 1870) and reports from other regions of
Europe (Rindi et al. 2004) and Asia (Krishnamurthy 2000; Neustupa 2003).
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Printzina cf. lagenifera (Hildebrand) Thompson & Wujek
This alga was collected from a concrete pillar supporting a small suspension bridge
at the resort of Storms River, Tsitsikamma National Park, South Africa, in September
2005. The material consisted of irregular masses with a pseudoparenchymatous habit,
producing a thin layer on the substratum, with no clear distinction between erect and
prostrate parts. The cells were globular, elliptical or barrel-shaped, 6-12 µm wide
(mainly 7-9) and 1-2 times as long as wide (Fig. 10). No reproductive structures
were observed.
The identification of the material described here must be regarded as somewhat
tentative. The vegetative morphology of the specimens is in agreement with that of
Printzina lagenifera, as generally described in the literature. It is widely accepted,
however, that this alga is very polymorphyc, showing a considerable range of variation
in colour, habit and branching pattern (Hariot 1889a; Nakano & Handa 1984; Rindi
& Guiry 2002a; Rindi et al. 2005). We believe that forms attributed to it are likely
to represent a complex of cryptic species with similar morphology; molecular data
will be necessary to clarify their relationships. Since no gametangia with elongated
neck (which is considered the diagnostic character of Printzina lagenifera) were
observed in the material collected, the specimens examined here cannot be separated
with certainty from similar species (for example Printzina ampla Thompson & Wujek;
Thompson & Wujek 1992) and are referred to this species only provisionally.
Printzina sp.
This alga formed an orange, thin mat on bark of trees on Zanzibar in April 2005.
The thallus appeared to consist primarily of a network of prostrate filaments from
which curved, irregularly branched erect axes were produced. These were, however,
densely compacted and produced a pseudoparenchymatous thallus, in which the
distinction between erect and prostrate parts was usually not clear (Figs 11, 12). The
cells varied greatly in shape; they were mainly globular, elliptical or barrel-shaped,
but in the erect axes they were often regularly cylindrical (Fig. 12). The cells were
7-17 µm wide (mainly 8-10), 1-2 times as long as wide; apical cells were longer (up
to 4 times as long as wide) and devoid of apical caps. Sporangiate laterals were
relatively common. The suffultory cell was produced in lateral or apical position,
either directly on the main axes or on short branchlets. The neck arose excentrically
and was comparatively long (Fig. 13); the zoosporangium was spherical, 10-16 µm
in diameter (Fig. 14). Although no empty sporangia could be observed, the ostiole
seemed to be opposite to the point of insertion.
In respect of the extensive development of the prostrate parts and the spherical shape
of the zoosporangium, this alga is clearly referable to Printzina. However, none of
the species included in this genus by Thompson & Wujek (1992) are in complete
agreement with the combination of habit, cell size, cell shape and sporangial
morphology observed for the Zanzibarian material. Printzina santurcensis (Tiffany)
Thompson & Wujek corresponds well to it for size and shape of the cells and
zoosporangia. However, the original description (Tiffany 1936, as Trentepohlia
santurcensis) and other reports on this species (Jose & Chowdary 1980; Thompson
437
Figs 10-17. Printzina cf. lagenifera, Printzina sp. and Trentepohlia abietina. Fig. 10. Printzina
cf. lagenifera. Detail of a fragment (scale = 20 µm). Figs 11-14. Printzina sp. Fig. 11. Habit (scale
= 50 µm). Fig. 12. Detail of thallus (scale = 30 µm). Fig. 13. A sporangiate lateral with immature
zoosporangium (scale = 10 µm). Fig. 14. Detail of a sporangiate lateral with zoosporangium (scale
= 10 µm). Figs 15-17. Trentepohlia abietina. Fig. 15. Habit of some erect axes (scale = 80 µm).
Fig. 16. Detail of an erect axis (scale = 20 µm). Fig. 17. Detail of a presumptive gametangium
(scale = 10 µm).
438
& Wujek 1992) did not provide many details on its habit and seem to suggest that
the erect parts are well developed and subdichotomously branched, which does not
agree with the morphology of the material from Zanzibar. As no currently recognized
species of Trentepohlia or Phycopeltis agree with this alga either, we believe that it
may represent an undescribed entity. We feel, however, that further collections
(possibly repeated in time) are desirable for a better characterization.
Trentepohlia abietina (Flotow) Hansgirg
Thin orange cushions referable to this alga were collected from bark of a palm tree
in the Durban Botanical Gardens in August 2005 and bark of an unidentified tree at
Stormy River, Eastern Cape, South Africa, in September 2005. The thallus consisted
of erect axes up to 400 µm tall, irregularly branched, arising from a limited system
of prostrate axes (Fig. 15). Cells of erect axes were cylindrical or sligthly swollen
(Fig. 16), 7-10 µm wide (mainly 7.5-8.0) and 1.5-5 times as long as wide (mainly
2-3). Cells of the prostrate parts were globular or elliptical, 8-12 µm in diameter. In
the Stormy River collection, the septa between adjacent cells showed great variation
in thickness; whereas some septa were much thicker than the adjacent lateral walls,
in other cases no noticeable difference was observed. No similar variation was observed
in the material from Durban, in which the septa were consistently thin. In both
collections the cell walls were ornamented by thin spiral strands, which could be
observed in detail only at high magnifications. Apical cells bore frequently a pectic
cap. Presumptive gametangia were the only reproductive structures observed. They
were borne on the erect axes in lateral or apical position; in the collection from
Durban, they often occurred in lateral series on 2-3 consecutive cells. At maturity
they were globular, 10-20 µm in diameter. In the collection from the Stormy River,
the wall was covered by thin scales (Fig. 17). No release of swarmers was observed.
Trentepohlia abietina is one of the most widespread species of the genus, having
been largely reported for many temperate and tropical regions throughout the world
(De Wildeman 1900; Jose & Chowdary 1980; Tracanna 1989; Ettl & Gärtner 1995;
John 2002; Rindi et al. 2005). This is the first documented record for Africa, although
the material reported by Printz (1920) as Trentepohlia aurea (Linnaeus) Martius is
probably referable to it. Despite reports suggesting the possible conspecificity of
Trentepohlia abietina and T. aurea (Hariot 1989b, 1890; Printz 1920; John 2002), in
our experience the morphology of T. abietina is generally stable and there is little
possibility of confusion with European specimens of T. aurea; recently, the taxonomic
separation of these species has been confirmed by molecular data (López-Bautista et
al. 2006). Several forms and varieties have been described for Trentepohlia abietina.
The morphology of the material from the Stormy River is in general agreement with
Trentepohlia abietina var. tenue, as characterized by Cribb (1970). This variety is
mainly distributed in tropical and subtropical regions and it differs from specimens
of Trentepohlia abietina from Europe and other temperate regions for the
ornamentation of the cell wall and the thickness of the septa (Cribb 1970). Our
specimens have a slightly larger cell width (7-10 µm, mainly 7.5-8.0) than the material
described by Cribb (1970) from Queensland (2-10 µm, mainly 5-8); the range of
variation, however, is comparable. The material from Durban is also close to the
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variety tenue, but it does not show the thickening of the septa reported as typical of
this taxon. It is not clear, however, how taxonomically relevant this character is, since
considerable variation was observed in the Stormy River material. In the past, great
importance has been attached to this feature and specimens from South-eastern Asia
with thick septa have been described as a separate species, Trentepohlia crassisaepta
Karsten (Karsten 1891). However, examination of the present collections and specimens
from other tropical localities (Rindi et al. 2005) has shown a wide range of variation in
the ornamentation of the cell wall and thickness of the septa; we therefore agree with
previous studies (Hariot 1889b; Cribb 1970) that these differences are probably not
relevant at the species level. Their possible taxonomic significance for delimitation of
intraspecific taxa needs to be assessed in combination with molecular data.
Trentepohlia afra (Massalongo) Cribb
Numerous specimens belonging to this species were discovered on 23 September 2005
on the Table Mountain (Cape Town, Western Cape, South Africa), growing as bright
orange tufts on shaded rocky surfaces. The tufts consisted of long erect axes, poorly
branched or unbranched (up to 1 cm tall), arising from a limited prostrate system (Fig.
18). The cells were regularly cylindrical, 20-30 µm wide (mainly 24-28), 2-4 times as
long as wide (Fig. 19); shape and size of the cells were similar in the erect and prostrate
parts. In healthy cells, the carotenoid pigments were abundant and dispersed into many
small, tiny droplets, which gave the alga a uniformly dark red colour when observed
microscopically. The cell walls were consistently thick, up to 5-6 µm, and finely
ornamented by numerous tiny strands, which gave the cell surface a corrugated
appearance (Fig. 20). Plasmodesmata between adjacent cells were very apparent, being
large and clearly protruding from each cell into the adjacent upper cell. The apical
cells were invariably provided with a thick pectic cap (Fig. 21); some were considerably
enlarged. Lateral branches arose as lateral protrusions from the top corners of cells.
Some intercalary cells were swollen, suggesting that restart of growth took place from
a larger apical cell. No reproductive structures were observed.
The vegetative morphology of Trentepohlia afra is very characteristic and it is
impossible to confuse with any other species, even in absence of reproductive
structures. Trentepohlia afra has long been considered conspecific with either
Trentepohlia flava (W.J.Hooker & Arnott) Cribb (= Trentepohlia polycarpa Nees &
Montagne) or Trentepohlia aurea (Hariot 1889c; Printz 1939). Cribb (1970), however,
considered that the larger size of the cells, the ornamentation, the thickness of the
wall and the habit of the apical caps distinguished this species from both T. aurea and
T. flava; we agree with his opinion. Chroolepus montis-tabulae Reinsch, based by
Reinsch (1877) on material from the Table Mountain in South Africa and transferred
by De Toni (1889) to Trentepohlia, is a later synonym for this species. Cribb (1970)
showed that Chroolepus afrum Massalongo (Massalongo 1861) is an earlier name for
this entity and based on it the new combination Trentepohlia afra. To date, the
known distribution of this species is restricted to Southern Africa. However, the fact
that it has usually been considered a synonym of other species makes it impossible to
assess with certainty its distributional range; it is possible that future collections will
reveal a much wider distribution.
440
Figs 18-23. Trentepohlia afra and Trentepohlia chinensis. Figs 18-21. Trentepohlia afra.
Fig. 18. Habit of an erect axis (scale = 500 µm). Fig. 19. Apical parts of erect axes (scale = 60 µm).
Fig. 20. Detail of cell walls (note superficial corrugation) (scale = 40 µm). Fig. 21. Detail of apical
cell with thick pectic cap (scale = 30 µm). Figs 22-23. Trentepohlia chinensis. Fig. 22. Habit of erect
axes (scale = 150 µm). Fig. 23. Detail of cells of erect axes (scale = 30 µm).
441
Trentepohlia chinensis (Harvey) Hariot
This alga was found in three separate collections, all obtained from tree bark: Zanzibar,
Tanzania, April 2005; Durban Botanical Gardens, South Africa, August 2005;
Tsitsikamma National Park, Eastern Cape, South Africa, 25 September 2005. This
species formed a dense brownish fur over the substratum. The thallus consisted of
long erect axes, up to 4 mm tall, arising from a scanty system of prostrate axes. The
erect axes were mostly unbranched in the sample from Tsitsikamma (Fig. 22); some
irregular and sparse branching occurred in the material from Zanzibar and Durban.
Cells were cylindrical, slightly inflated or barrel-shaped, 12-25 µm wide (Fig. 23);
with regard to this character, the material from Durban showed a larger range of
variation (12-25 µm) than the populations from Zanzibar and Tsitsikamma
(20-25 µm). In the specimens from Tsitsikamma the width:length ratio was higher
(cells 1.5-3 times as long as wide, mainly 2-2.5) than in the collections from Durban
and Zanzibar (cells 1-3 times as long as wide, mainly 1.2-1.8). When present, lateral
branches arose in the middle of the cells and were borne at a 90° angle (Fig. 24).
Apical cells were blunt, dome-shaped, and no apical caps were observed. Cells of
the prostrate parts were similar in size and shape to those of the erect axes.
Plasmodesmata between adjacent cells were often very obvious. Large amounts of
carotenoid pigments occurred in the material from Tsitsikamma, in which they showed
a characteristic distribution, forming numerous small droplets arranged in a parietal
layer. The production of these pigments seemed to be associated with the chloroplasts
(which, when observable, looked like small parietal plates forming a more or less
extensive network). Characteristically, in many cells the layer of carotenoid pigments
was not uniform, giving the impression of one or more holes (Fig. 25). Fungal
hyphae were commonly mixed with the alga, especially in the collection from Durban.
No reproductive structures were observed in any collection.
Trentepohlia chinensis was based by Hariot (1889b) on Chroolepus chinensis Harvey,
described by Harvey (1860) for material collected from rocks in Hong Kong. The
morphological characterization of this species is problematic. Harvey’s (1860) original
description is brief and does not mention several features that are important in the
infrageneric taxonomy of Trentepohlia. Hariot (1889b) examined authentic material
of this species and provided additional information, including cell size, new records
and illustrations of a specimen from Madagascar. Cribb (1970), however, examined
the type specimen and remarked on some discrepancies between its morphology and
the description of Hariot (1889b). In particular, he noted that the width: length ratio
of the cells was longer than reported by Hariot and that the filaments tapered distinctly
Figs 24-31. Trentepohlia chinensis, Trentepohlia flava and Trentepohlia umbrina. Figs 24-25. Trentepohlia chinensis. Fig. 24. Detail of branching (scale = 50 µm). Fig. 25. Detail of cell pigmentation
(scale = 20 µm). Figs 26-29. Trentepohlia flava. Fig. 26. Habit of erect axes (scale = 40 µm).
Fig. 27. Detail of erect axes showing corrugation of the cell walls (scale = 40 µm). Fig. 28. Detail of
prostrate parts (scale = 40 µm). Fig. 29. Detail of a presumptive gametangium, containing unreleased
presumptive gametes (scale = 20 µm). Figs 30-31. Trentepohlia umbrina. Fig. 30. Habit (scale = 20 µm).
Fig. 31. Upper view of a presumptive gametangium (note ostiole in the centre) after release of
presumptive gametes (scale = 20 µm).
442
443
towards the apex, which is clearly not the case in the figure of Hariot (1889b: 379).
Cribb (1970) concluded that, if the figure is typical of Hariot’s concept of Trentepohlia
chinensis, it is unlikely to represent the same species as the type specimen; he therefore
regarded this species as a doubtful entity. In our opinion, the three collections from
Africa examined in this study are clearly representative of the same taxon, and Hariot’s
Trentepohlia chinensis is the species to which they are morphologically closest. The
examination of our samples suggests that this alga is polymorphic and several features
(development of branching, cell width, length:width ratio of cells) are subjected to
a relatively wide range of variation. It looks therefore possible that Harvey’s type
material and Hariot’s alga represent different morphological variants of the same
entity. Further collections, combined with culture studies, are necessary to understand
better the morphological variability of this species; in particular, examination of
reproductive material is much needed. We agree with Cribb (1970) that, until further
collections from the type locality become available, the relationship between the
Chinese and the African populations needs reassessment. We also agree that this
species is very similar to Trentepohlia arborum (C.Agardh) Hariot. Habit, branching
pattern and cell size are virtually identical in the two species, although Trentepohlia
arborum usually has a lighter colour, apical cells attenuated and a generally higher
length:width cell ratio (Printz 1939; Islam 1960; Cribb 1970; Rindi et al. 2005).
Trentepohlia flava (W.J.Hooker & Arnott) Cribb
This species formed a velvety coating on stems and leaves of shrubs and trees in the
coastal region of Swakopmund, Namibia, in July 2005. It was also collected from
the painted concrete wall of a cottage-like building in the De Hoop Nature Reserve,
Western Cape, South Africa, on 3 October 2005. The alga consisted of erect axes, up
to 700-800 µm tall, arising from a well-developed system of prostrate filaments.
The erect filaments were straight or curved, poorly branched or unbranched
(Fig. 26). When present, branches mainly occurred in the lower parts, without a
regular arrangement; branches with Scytonema-like appearance were observed
occasionally. New branches were issued as protrusions from the top corner of the
cells. In the material from Swakopmund the prostrate filaments were loose, whereas
in the sample from De Hoop the basal part consisted of strictly entangled filaments
forming a compact, almost pseudoparenchymatous layer. In the erect parts, the cells
were cylindrical or slightly inflated, 10-20 µm wide (mainly 15-18 for Swakopmund,
14-16 for De Hoop), 1-3 times as long as wide (Fig. 27). Most cells of the erect axes
had a thick cell wall (up to 5 µm), heavily corrugated by spiral strands and scales.
Apical cells were either blunt or sharpened, with a variably developed cap. Whereas
in the sample from Swakopmund the cells of the prostrate parts were similar in
shape and size to those of the erect parts, in the material from De Hoop they were
mostly globular or elliptical, 13-20 µm in diameter (Fig. 28); for both samples, the
corrugation observed in the erect parts was either absent or weakly developed.
Presumptive gametangia were observed in the sample from De Hoop. They were
globular or urn-shaped, 20-25 µm in diameter, and occurred either terminally at the
top of the erect axes or in intercalary position (Fig. 29). Some sporangiate laterals,
produced either on apical cells or at the top of short lateral branches, were observed
in the sample from Swakopmund. The zoosporangia were globular or subglobular,
444
20-30 µm in diameter, with the ostiole opposite to the attachment. The neck of the
suffultory cell was initially straight, but in fully developed sporangiate laterals it
was more or less markedly bent.
Considerable uncertainty has long surrounded the exact circumscription of this species,
which is mostly reported in the literature as Trentepohlia polycarpa Nees & Montagne
or Trentepohlia aurea var. polycarpa (Nees & Montagne) Hariot. By examination of a
large number of relevant herbarium specimens, Cribb (1970) reassessed its taxonomic
position and geographical distribution, and renamed it Trentepohlia flava. Our specimens
are generally in good agreement with the morphological characterization provided by
this author and we largely agree with his conclusions. Our records, however, show that
this species is not strictly confined to America, as believed by Cribb. It is noteworthy
that several documented records confirmed by Cribb (1970: 18) exist for some of the
southernmost regions of America (Patagonia, Tierra del Fuego, Strait of Magellan and
Falkland Islands). The presence of Trentepohlia flava in southern Africa, which in past
geological eras has been connected to such parts of South America, is therefore not
particularly surprising. The samples from Namibia and South Africa represent the first
documented records of this species for Africa. Hariot (1889c: 373) mentioned a record
(as Trentepohlia polycarpa) from Cape of Good Hope; however, in consideration of
Hariot’s incorrect circumscription of this species (see discussion in Cribb 1970), this
record cannot be confirmed.
Trentepohlia umbrina (Kützing) Bornet
Material attributable to this species was found in three collections. In one from
Zanzibar and one from Tsitsikamma National Park, South Africa, the alga formed a
brownish-orange mat on tree bark; in one from Plettenberg Bay, South Africa, it
formed small dark red masses, with more or less hemispherical to irregular shape,
on natural rocks. Thalli of this species consisted of many entangled filaments, forming
compact masses without a distinction between erect and prostrate parts. When
removed, the thalli were easily fragmented into short filaments. The cells varied in
shape from globular to almost cylindrical, but were mostly subglobular or elliptical
(Fig. 30). They were 9-25 µm wide; the material from Zanzibar was more robust
(mainly 18-22 µm), than the material from South Africa (mainly 10-14 µm). In the
population from Zanzibar, the cell walls were finely ornamented by many small dotlike protrusions. Presumptive gametangia were present in the population from
Zanzibar (Fig. 31); they were globular, 20-26 µm in diameter and, during microscopical observation, they released large numbers of biflagellate, presumptive gametes,
which were not observed to fuse. No reproductive structures were observed in the
material from South Africa.
Trentepohlia umbrina is one of the most widespread species of the genus; records
exist for almost all regions of the world where Trentepohliales have been collected.
The morphology of this species is generally stable and its identification is usually
straightforward, although its exact separation from Trentepohlia odorata has been
source of controversy in the past (Hariot 1989a). The original collections of this
species (as Chroolepus umbrinum Kützing; Kützing 1843) were made from tree bark
in southern Germany and the occurrence on this type of substratum is considered an
445
important character for its identification (Printz 1939, 1964). Recent investigations,
however, have shown that material referable to this species also occurs on stone and
artificial surfaces (Rindi & Guiry 2002a; Rindi et al. 2003; present study). With
regard to morphology, there is no basis for a different taxonomic attribution of
populations occurring on tree bark from populations occurring on stone; nevertheless,
a confirmation of the genetic identity of different populations based on molecular
methods is desirable.
The new records documented in this study include trentepohlialean taxa with
pantropical (Phycopeltis arundinacea, P. epiphyton, Trentepohlia abietina, T. umbrina)
and endemic distributions (Trentepohlia afra), and other taxa for which the uncertain
delimitation at the species level precludes a precise assessment of the distribution
(Printzina sp., Trentepohlia chinensis, T. flava). The phylogeography of the
Trentepohliales represents an interesting evolutionary puzzle; its clarification is
presently prevented by poor understanding of the taxonomic and evolutionary
relationships among members of this group. A detail taxonomic assessment at species
and genus level, based on a combination of morphological, molecular and
physiological data and a careful examination of many herbarium specimens, is
essential to clarify phylogeographic patterns in this order. We are currently analysing
the evolutionary history of this group by phylogenetic analyses based on sequences
of several molecular markers; such data are essential for testing hypotheses concerning
biogeographic patterns, clarifying the taxonomy of problematic taxa (e.g., the
Printzina lagenifera complex) and assessing in detail the taxonomic identity and
distribution of some species that are currently regarded as widespread. Such
information will provide a framework that will be of great importance to understand
the evolution and biogeography of other groups of subaerial algae; it will also be
particularly valuable because the Trentepohliales have their centre of diversity in
tropical and subtropical regions. Humid tropical and subtropical forests host a large
number of habitats that are favourable for the development of a rich and diverse
subaerial algal flora. The information available on subaerial algae of tropical regions
is generally limited and, in particular, very little is known about algae of tropical
rainforests. This is particularly worrying both because these are among the most
endangered ecosystems on the planet and because recent investigations have shown
that many new taxa, including some major evolutionary surprises, can be expected
to be discovered in these environments (Neustupa 2003, Neustupa & Sejnohová
2003, Neustupa 2005, Rindi et al. 2006). Algal and microbial communities of tropical
and subtropical forests represent an untapped biological resource for studies on
systematics and evolution, and a better knowledge of their diversity is urgently needed.
Acknowledgements
We are very grateful to Dr Willem Prud’homme van Reine (Rijksherbarium, Leiden, the Netherlands)
for providing the collection of Trentepohlia flava from Namibia. JMLB and FR acknowledge financial
support by the National Science Foundation (Systematics Program DEB-0542924). MDG’s
collections in South Africa and Tanzania were made in the course of surveys for which travel
expenses were partially funded by the European Commission, under an International Scientific
Cooperation Project (SEAWEEDAFRICA, contract ICA4-CT-2001-10030).
446
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